FN Archimer Export Format
PT J
TI Wind ringing of the ocean in presence of mesoscale eddies
BT 
AF KLEIN, Patrice
   LAPEYRE, Guillaume
   LARGE, WG
AS 1:;2:;3:;
FF 1:;2:;3:;
C1 IFREMER, Lab Phys Oceans, Plouzane, France.
   NCAR, Climate & Global Dynam Div, Boulder, CO USA.
C2 IFREMER, FRANCE
   NCAR NATL CTR ATMOSPHER RES, USA
SI BREST
SE PDG-DRO-DOPS-LPO
IN WOS Ifremer jusqu'en 2018
   copubli-int-hors-europe
IF 2.378
TC 35
UR https://archimer.ifremer.fr/doc/00000/10838/9262.pdf
LA English
DT Article
AB Recent findings have highlighted the impact of high frequency (HF) winds on the inertial motions and the consequences on the large-scale oceanic circulation [Wunsch and Ferrari, 2004]. Within this context the present study focuses on the role of intermediate scales related to oceanic mesoscale eddies. Results show that a turbulent eddy field does not affect the impact of HF winds on the inertial motions. However the eddies efficiently and permanently concentrate the wind-forced inertial motions in small-scale anticyclonic structures. This leads to a spatially heterogeneous vertical mixing strongly related to the eddy field properties.
PY 2004
PD AUG
SO Geophysical Research Letters
SN 0094-8276
PU Amer Geophysical Union
VL 31
IS 15
UT 000223335600005
BP 1
EP 4
DI 10.1029/2004GL020274
ID 10838
ER

EF